V. Degrange et al., NITRIFICATION AND OCCURRENCE OF NITROBACTER BY MPN-PCR IN LOW AND HIGH NITRIFYING CONIFEROUS FOREST SOILS, Plant and soil, 198(2), 1998, pp. 201-208
The nitrification of three coniferous forest soils was investigated: a
podzol (Fontainebleau, France) with low N deposition and no nitrate a
ccumulation, an acid mull (Haldon, UK) with low N deposition and moder
ate nitrate accumulation, and a podzol (Wekerom, The Netherlands) with
high N deposition and high nitrate accumulation. Twenty-one months in
situ lysimeter experiments and short-term and long-term in vitro incu
bations were performed to respectively establish the status of NO3- ac
cumulation and potential nitrification of these soils. These complemen
tary approaches allowed to conclude that the absence of NO3- accumulat
ion in Fontainebleau soil was effectively due to a lack of nitrifing a
ctivity in the whole profile while the high NO3- accumulation observed
in the Wekerom soil essentially resulted from an active nitrifying ac
tivity in the Oh horizon of this soil. For the Haldon soil, the inadeq
uacy between the lysimeter and the short-term in vitro experiment was
discussed. Surprisingly, relatively high densities of the nitrite-oxid
iser Nitrobacter (enumerated by PCR-MPN technique) were found in all t
he studied horizons of the three soils. Moreover, a long-term incubati
on experiment showed that inhibition of nitrification in the Oh Fontai
nebleau soil could be removed after submitting the soil samples to con
stant conditions during 82 days. This demonstrates that in these soils
, ammonium-oxidisers (as well as nitrite-oxidisers) are present and th
at extrinsic factors were involved in the inhibition of nitrification.